Internal and forced climate variability during the last millennium: a model-data comparison using ensemble simulations

By Hugues Goosse, Hans Renssen, A. Timmermann, R. Bradley. 2005

222 citations recorded by the source corpus.

Subfields: Atmospheric Science, Paleontology

View Paper: https://www.semanticscholar.org/paper/39d4562744c281e71a28db93caa1359c74a2c469

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Hans Renssen
2. Hugues Goosse
3. Stefan Rahmstorf
4. A. Timmermann
5. Svetlana Jevrejeva
6. Aslak Grinsted
7. John C. Moore
8. R. Muscheler

In Paleontology

1. Martin Vermeer
2. Stefan Rahmstorf
3. Hans Renssen
4. Hugues Goosse

Citations in the corpus

• Millennial temperature reconstruction intercomparison and evaluation (2006, unknown): “The results of Weber et al. (2004) and Goosse et al. (2005) suggest that such estimates of regional mean temperatures can provide some information about global mean anomalies, as they strongly reflect the external forcings on centennial and longer timescales.”
• Reconstructing surface temperature changes over the past 600 years using climate model simulations with data assimilation (2010, methodology): “ferent data set (surface temperature obtained from thermometers) but the same methodology, Goosse et al. [2009] successfully reproduced the year‐to‐year variations in tem-”
• Description of the Earth system model of intermediate complexity LOVECLIM version 1.2 (2010, methodology): “…Menviel, 2008; Menviel et al., 2008), the last deglaciation (e.g. Timm et al., 2009), the Holocene climate (e.g., Renssen et al., 2001, 2003, 2005; Jiang et al., 2005), the previous interglacials (e.g., Duplessy et al., 2007; Yin et al., 2008), the last millennium (e.g., Goosse et al., 2005; van…”
• The role of forcing and internal dynamics in explaining the “Medieval Climate Anomaly” (2011, methodology): “In addition, the internal variability of the system, purely driven by its own dynamics, can also be responsible for some of the reconstructed changes, in particular at regional scale (Goosse et al. 2005a; Servonnat et al. 2010).”
• How will sea level respond to changes in natural and anthropogenic forcings by 2100? (2010, methodology): “We therefore created our own scenario for the 21st century based on the most extreme century of volcanic radiative forcing over the last 1000 years (the 13th century) [Crowley et al., 2003; Goosse et al., 2005].”
• Coupled climate model simulation of Holocene cooling events: oceanic feedback amplifies solar forcing (2006, background): “…and Renssen, 2006), solar forcing of climate change (Goosse et al., 2002; van der Schrier et al., 2002; Goosse and Renssen, 2004; Weber et al., 2004), the climate of the last millennium (Goosse et al., 2004; Goosse et al., 2005a, b) and future climate evolution (Schaeffer et al., 2002, 2005).”
• Global sea level linked to global temperature (2009, methodology): “A good performance is also found for millennial simulations with two other climate models, the ECHO-G model (6) and the ECBilt-CLIO model (14) (see S3 and S4 in SI Appendix).”